Column study reveals that low-molecular-weight aliphatic acids enhance sulfate mobility in forested Cecil soil, suggesting organic acids regulate nutrient retention and leaching.
Dissolved organic substances derived from forest litter are believed to influence the retention and movement of SO 2− 4 in forest soils. A column study was conducted in which 35 SO 4 was surface applied to a soil and leached with either low‐molecular‐weight aliphatic acids (AA) or a forest‐litter extract. Oxalic, malonic, and succinic acids were used in the concentration range 8.0 × 10 −3 to 1.0 × 10 −5 mol L −1 . Movement of 35 SO 4 was determined with column depth, as was the 35 SO 4 activity in the collected leachates. Labeled SO 4 soil movement was found to increase with increasing AA concentration. Leachate 35 SO 4 activity was observed to increase in the order malonic > succinic > oxalic for acid treatments > 1.0 × 10 −4 mol L −1 . The 1.0 × 10 −5 mol L −1 acid treatments did not result in 35 SO 4 break‐through in the soil columns. Reduced exchangeable 35 SO 4 for organic acid ≥ 1.0 × 10 −3 mol L −1 suggests that at high concentrations, aliphatic acids may activate sulfate retention sites in soil, while at lower concentrations these acids may accelerate the movement of 35 SO 4 in forest soils due to selective organic‐acid adsorption by soil components.
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Evans et al. (1990) studied this question.
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